Plate Margins 5.0 / 5 based on 1 rating ? GeographyRock landscapes and processesGCSEAQA Created by: JonathenCreated on: 27-03-13 19:18 24315 Across 1. 2 continental plate. Move apart from each other. Earthquakes friction moving over mantle. Eruptions. Cracks under ground called Fissures. (12) Down 2. Oceanic and Continental Crust. Oceanic subducts denser. Friction between two plates causes Earthquakes. Land on the edge of Continental Crust is compressed to form Fold Mountains. (11) 3. Older 1500 years old. Thicker and more dense. Cannot be destroyed and renewed. (11) 4. Two plates moving side by side, creates friction therefore this creates Earthquakes. Different directions or same direction at different speeds. (12) 5. Newer 200 million years old. Denser. Thinner. Can be destroyed and renewed. (7)
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